Evaluation of the long-term effect of biochar on properties of temperate agricultural soil at pre-industrial charcoal kiln sites in Wallonia, Belgium

Hardy, Brieuc;Cornelis, Jean-Thomas;Houben, David;Leifeld, J;Dufey, Joseph;et.al.
(2016) European Journal of Soil Science — n° 68, p. 80-89 (2017)

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Authors
  • Hardy, BrieucUCLouvain
    Author
  • Cornelis, Jean-ThomasGemblouxAGROBIOTECH
    Author
  • Houben, DavidInstitut_Polytechique_LaSalle_Beauvais_France
    Author
  • Leifeld, JInstitute_for_Sustainability_Sciences_Zürich_Switzerland
    Author
  • Author
  • Dufey, JosephUCLouvain
    Author
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Abstract
Research on biochar has increased, but its long-term effect on the fertility of temperate agricultural soil remains unclear. InWallonia, Belgium, pre-industrial charcoal production affected former forested areas that were cleared for cultivation in the nineteenth century. The sites of traditional charcoal kilns, largely enriched in charcoal residues, are similar to soil amended with hardwood biochar more than 150 years ago. We sampled 17 charcoal kiln sites to characterize their effect on soil properties compared with adjacent reference soils. Charcoal-C content was estimated by differential scanning calorimetry. The kiln soil contains from 1.8 to 33.1 g kg−1 of charcoal-C, whichmarkedly increases organic C:N and C:P ratios. It also contains slightly more uncharred soil organic carbon (SOC) than the reference soil, which accords with larger total N content.We measured a small increase in nitrates in the kiln soil that might relate to greater mineralization and nitrification of organic N. Frequent application of lime raised the pH to values close to neutral, which offset the residual effect of charcoal production on soil acidity. A cation exchange capacity (CEC) of 414 cmolc kg−1 was estimated for charcoal-C, whereas that of uncharred SOC was 213 cmolc kg−1. Despite the large CEC of the kiln soil, exchangeable K+ content was no different from the adjacent soil, whereas exchangeable Ca2+ and Mg2+ contents were considerably larger. Charcoal enrichment has little effect on available, inorganic and total P, but it can form strong complexes with Cu, which reduces the availability of the metal. Biochar is very persistent in soil; therefore, long-term implications should not be overlooked.
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Citations

Hardy, B., Cornelis, J.-T., Houben, D., Leifeld, J., Lambert, R., & Dufey, J. (2016). Evaluation of the long-term effect of biochar on properties of temperate agricultural soil at pre-industrial charcoal kiln sites in Wallonia, Belgium. European Journal of Soil Science, 68, 80-89. https://doi.org/10.1111/ejss.12395 (Original work published 2017)